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青岛胶州湾3.2级地震构造背景与控震断裂
引用本文:栾光忠,刘红军,刘冬雁.青岛胶州湾3.2级地震构造背景与控震断裂[J].中国海洋大学学报(自然科学版),2002,32(5):763-769.
作者姓名:栾光忠  刘红军  刘冬雁
作者单位:青岛海洋大学海洋地球科学学院,青岛,266003
摘    要:本文应用构造分析的方法 ,对青岛胶州湾 3.2级地震发生的地震地质背景和构造背景进行分析。结果表明 :胶州湾 3.2级地震主要受 NEE向郝官庄断裂和 NNW向大沽河断裂控制 ,并根据现代活动断裂的标志 ,对上述 2组断裂活动性特征作了阐述

关 键 词:青岛胶州湾  地震  构造地质背景  控震断裂  城市环境地质
文章编号:1001-1862(2002)05-0763-07
修稿时间:2002年3月4日

The Background of Seismic Structure and Controlled-Earthquake Faults of 3.2 Grade Earthquake in Jiaozhou Bay of Qingdao
Luan Guangzhong\ Liu Hongjun\ Liu Dongyan.The Background of Seismic Structure and Controlled-Earthquake Faults of 3.2 Grade Earthquake in Jiaozhou Bay of Qingdao[J].Periodical of Ocean University of China,2002,32(5):763-769.
Authors:Luan Guangzhong\ Liu Hongjun\ Liu Dongyan
Abstract:By using the method of geologic structural analysis, the backgroung of seismic structure and the controlled earthquake faults of 3.2 grade earthquake in Jiaozhou Bay are studied. It is assumed that the earthquake was mainly controlled by the Haoguanzhuang fault and Daguhe fault which run in the NEE and NNW direction respectively. Based on the marks of modern movements of fractures, the characteristics of the two faults are expounded.
Keywords:Jiaozhou Bay of Qingdao  earthquake  background of structural geology  controlled  earthquake faults  city evironment geology
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